The connection between trends of mean temperature and circulation at the surface: Part III. Spring

Jill Williams; Harry van Loon

doi:10.1175/1520-0493(1976)104<1591:TCBTOM>2.0.CO;2

The connection between trends of mean temperature and circulation at the surface: Part III. Spring

Jill Williams, Harry van Loon

Climatic Research Unit

Research output: Contribution to journal › Article › peer-review

Abstract

The sign of the weighted temperature change over two periods (1950–64, 1942–72) for 15°–80°N was determined by the change in the polar region in spring and autumn, as it was in winter but not in summer. Each of the four seasons shows a different distribution of zonally averaged temperature changes.

Original language	English
Pages (from-to)	1591-1596
Number of pages	6
Journal	Monthly Weather Review
Volume	104
Issue number	12
DOIs	https://doi.org/10.1175/1520-0493(1976)104<1591:TCBTOM>2.0.CO;2
Publication status	Published - 1976

Access to Document

10.1175/1520-0493(1976)104<1591:TCBTOM>2.0.CO;2

Cite this

@article{26400ad62efd4e9d86f614c9f8b684ff,

title = "The connection between trends of mean temperature and circulation at the surface: Part III. Spring",

abstract = "The sign of the weighted temperature change over two periods (1950–64, 1942–72) for 15°–80°N was determined by the change in the polar region in spring and autumn, as it was in winter but not in summer. Each of the four seasons shows a different distribution of zonally averaged temperature changes.",

author = "Jill Williams and {van Loon}, Harry",

year = "1976",

doi = "10.1175/1520-0493(1976)104<1591:TCBTOM>2.0.CO;2",

language = "English",

volume = "104",

pages = "1591--1596",

journal = "Monthly Weather Review",

issn = "0027-0644",

publisher = "American Meteorological Society",

number = "12",

}

TY - JOUR

T1 - The connection between trends of mean temperature and circulation at the surface: Part III. Spring

AU - Williams, Jill

AU - van Loon, Harry

PY - 1976

Y1 - 1976

N2 - The sign of the weighted temperature change over two periods (1950–64, 1942–72) for 15°–80°N was determined by the change in the polar region in spring and autumn, as it was in winter but not in summer. Each of the four seasons shows a different distribution of zonally averaged temperature changes.

AB - The sign of the weighted temperature change over two periods (1950–64, 1942–72) for 15°–80°N was determined by the change in the polar region in spring and autumn, as it was in winter but not in summer. Each of the four seasons shows a different distribution of zonally averaged temperature changes.

U2 - 10.1175/1520-0493(1976)104<1591:TCBTOM>2.0.CO;2

DO - 10.1175/1520-0493(1976)104<1591:TCBTOM>2.0.CO;2

M3 - Article

VL - 104

SP - 1591

EP - 1596

JO - Monthly Weather Review

JF - Monthly Weather Review

SN - 0027-0644

IS - 12

ER -